吉林延边五凤地区早侏罗世粗面安山岩岩石成因

doi:10.13686/j.cnki.dzyzy.2024.01.002

Abstract
Figure/Table
References
Related Citation (15)

Download: PDF (986 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS)

Abstract Study on the petrology, LA-ICP-MS zircon U-Pb dating and whole rock geochemistry of the trachyandesite in Wufeng area of Yanbian, Jilin Province in Northeast China, shows that the SiO₂ content is 58.33%-61.36%, K₂O content 1.61%-3.28% and total alkali content 6.77%-10%, belonging to the medium potassium-high potassium calc-alkaline series. The weighted mean age of magmatic zircon ²⁰⁶Pb/²³⁸U is 175.52±2.7 Ma, which is consistent with the subduction time of Early Jurassic paleo-Pacific plate. The trachyandesite is characterized by relative enrichment of LILEs(K, Ba and Rb) and strongly incompatible elements (Th and U), and depletion of HFSEs (Nb, Ta and Ti), with high LREE/HREE ratio, and enriched LREEs and depleted HREEs, indicating that the magma may originate from the partial melting of mantle and its source area is metasomatized by the subducted shell source materials. From the above, it is believed that the trachyandesite was formed in the active continental margin of oceanic subduction system and was the magmatic response to the subduction of Early Jurassic paleo-Pacific plate.

Key words： trachyandesite lithogeochemistry zircon U-Pb age paleo-Pacific plate Early Jurassic active continental margin Jilin Province

Received: 28 November 2022

PACS:	P595
	P597

About author:: 10.13686/j.cnki.dzyzy.2024.01.002

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	GAO Zi-yue
	JU Nan
	LI Jing-wei
	YANG Qun
	WANG Ke-yong

Cite this article:

GAO Zi-yue,JU Nan,LI Jing-wei等. PETROGENESIS OF THE EARLY JURASSIC TRACHYANDESITE IN WUFENG AREA OF YANBIAN, JILIN PROVINCE[J]. GEOLOGY AND RESOURCES, 2024, 33(1): 12-23,40.

URL:

http://manu25.magtech.com.cn/Jweb_dzyzy/EN/10.13686/j.cnki.dzyzy.2024.01.002 OR http://manu25.magtech.com.cn/Jweb_dzyzy/EN/Y2024/V33/I1/12

[1]	邵济安, 牟保磊, 何国琦, 等. 华北北部在古亚洲域与古太平洋域构造叠加过程中的地质作用[J]. 中国科学(D辑), 1997, 27(5): 390-394. Shao J A, Mu B L, He G Q, et al. Geological effects in tectonic superposition of Paleo-Pacific domain and Paleo-Asian domain in northern part of North China[J]. Science in China Series D:Earth Sciences, 1997, 40(6):634-640.
[2]	李锦轶. 中国东北及邻区若干地质构造问题的新认识[J]. 地质论评, 1998, 44(4):339-347. Li J Y. Some new ideas on tectonics of NE China and its neighboring areas[J]. Geological Review, 1998, 44(4):339-347.
[3]	唐克东, 鞠楠, 张大权, 等. 关于古亚洲洋构造演化研究的几点思考[J]. 地质与资源, 2022, 31(3):246-258, 330. Tang K D, Ju N, Zhang D Q, et al. Implication of the tectonic evolution of Paleo-Asian Ocean[J]. Geology and Resources, 2022, 31(3):246-258, 330.
[4]	冯亚洲, 杨进辉, 孙金凤, 等. 中生代古太平洋板块俯冲诱发华北克拉通破坏的物质记录[J]. 中国科学:地球科学, 2020, 50(5): 651-662. Feng Y Z, Yang J H, Sun J F, et al. Material records for Mesozoic destruction of the North China Craton by subduction of the Paleo- Pacific slab[J]. Science China Earth Sciences, 2020, 63(5):690- 700.
[5]	赵春荆. 吉黑东部构造格架及地壳演化[M]. 沈阳:辽宁大学出版社, 1996:136-138. Zhao C J. Tectonic framework and crust evolution of eastern Jilin and Heilongjiang provinces[M]. Shenyang:Liaoning University Press, 1996:136-138.
[6]	芮宗瑶, 张洪涛, 王龙生, 等. 吉林延边地区斑岩型-浅成热液型金铜矿床[J]. 矿床地质, 1995, 14(2):99-126. Rui Z Y, Zhang H T, Wang L S, et al. Porphyry-epithermal copper- gold deposits in Yanbian area, Jilin Province[J]. Mineral Deposits, 1995, 14(2):99-126.
[7]	Goldfarb R J, Mao J W, Qiu K F, et al. The great Yanshanian metallogenic event of eastern Asia:Consequences from one hundred million years of plate margin geodynamics[J]. Gondwana Research, 2021, 100:223-250.
[8]	Goldfarb R, Qiu K F, Deng J, et al. Orogenic gold deposits of China [C]//Chang Z S, Goldfarb R J. Mineral Deposits of China. Society of Economic Geologists Special Publication, 2019:263-324.
[9]	贾大成, 胡瑞忠, 冯本智, 等. 吉林延边地区中生代火山岩金铜成矿系列及区域成矿模式[J]. 长春科技大学学报, 2001, 31(3):224- 229. Jia D C, Hu R Z, Feng B Z, et al. Gold-copper metallogenic series and metallogenic model of Mesozoic volcanic belt in Yanbian area, Jilin Province[J]. Journal of Changchun University of Science and Technology, 2001, 31(3):224-229.
[10]	Jia D C, Hu R Z, Lu Y, et al. Collision belt between the Khanka block and the North China block in the Yanbian region, Northeast China[J]. Journal of Asian Earth Sciences, 2004, 23(2):211-219.
[11]	吉林省地质矿产局. 吉林省区域地质志[M]. 北京:地质出版社, 1988:202-205. Bureau of Geology and Mineral Resources, Jilin Province. Regional geological records of Jilin Province[M]. Beijing:Geological Publishing House, 1988:202-205. (in Chinese)
[12]	殷长建, 彭玉鲸, 靳克. 中国东北东部中生代火山活动与泛太平洋板块[J]. 中国区域地质, 2000, 19(3):303-311. Yin C J, Peng Y J, Jin K. Mesozoic volcanism in the eastern part of Northeast China and Transpacific plate[J]. Regional Geology of China, 2000, 19(3):303-311.
[13]	李超文, 郭锋, 范蔚茗, 等. 延吉地区晚中生代火山岩的Ar-Ar年代学格架及其大地构造意义[J]. 中国科学D辑:地球科学, 2007, 37(3):319-330. Li C W, Guo F, Fan W M, et al. Ar-Ar geochronology of Late Mesozoic volcanic rocks from the Yanji area, NE China and tectonic implications[J]. Science in China Series D:Earth Sciences, 2007, 50(4):505-518.
[14]	纪伟强. 吉黑东部中生代晚期火山岩的年代学和地球化学[D]. 长春:吉林大学, 2004. Ji W Q. Chronology and geochemistry of late Mesozoic volcanic rocks in eastern Jilin and Heilongjiang Provinces[D]. Changchun:Jilin University, 2004.
[15]	陈聪. 延边东部晚古生代-中生代构造演化与区域成矿规律[D]. 长春:吉林大学, 2017. Chen C. Late Paleozoic-Mesozoic tectonic evolution and regional metallogenic regularity of the eastern Yanbian area, NE China[D]. Changchun:Jilin University, 2017.
[16]	门兰静, 孙景贵, 陈雷, 等. 延边地区五凤-五星山金矿床成矿流体与成矿作用研究[J]. 矿床地质, 2016, 35(2):381-394. Men L J, Sun J G, Chen L, et al. Ore-forming fluid and mineralization of Wufeng-Wuxingshan gold deposit, Yanbian area[J]. Mineral Deposits, 2016, 35(2):381-394.
[17]	张艳斌. 延边地区花岗质岩浆活动的同位素地质年代学格架[D]. 长春:吉林大学, 2002. Zhang Y B. Isotopic geochronology framework of granitic magmatic activity in Yanbian area[D]. Changchun:Jilin University, 2002. (in Chinese)
[18]	张笑鸣. 华北克拉通东北缘中生代岩浆事件——对多构造体系演化的制约[D]. 长春:吉林大学, 2021. Zhang X M. Mesozoic magmatic events in the northeastern margin of the North China Craton:Constraints on the evolution of the multiple tectonic regimes[D]. Changchun:Jilin University, 2021.
[19]	赵羽军, 孙景贵, 王清海, 等. 吉林延边地区浅成热液金(铜)矿床的40Ar/39Ar激光探针测年与成矿时代讨论[J]. 地学前缘, 2010, 17(2):156-169. Zhao Y J, Sun J G, Wang Q H, et al. 40Ar/39Ar laser probe dating and discussion on metallogenic epoch of epithermal Au-Cu deposit in Yanbian area of Jilin[J]. Earth Science Frontiers, 2010, 17(2): 156-169.
[20]	刘金龙, 孙丰月, 林博磊, 等. 吉林延边闹枝金矿区粗面安山岩锆石U-Pb年代学、地球化学特征及其构造意义[J]. 吉林大学学报(地球科学版), 2015, 45(5):1394-1404. Liu J L, Sun F Y, Lin B L, et al. Geochronology and geochemistry of trachyandesite of Naozhi gold deposit in Yanbian region, southern Jinlin Province and its geological significance[J]. Journal of Jilin University (Earth Science Edition), 2015, 45(5):1394-1404.
[21]	Middlemost E A K. Naming materials in the magma/igneous rock system[J]. Earth-Science Reviews, 1994, 37(3/4):215-224.
[22]	Maniar P D, Piccoli P M. Tectonic discrimination of granitoids[J]. GSA Bulletin, 1989, 101(5):635-643.
[23]	Peccerillo A, Taylor S R. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976, 58(1):63-81.
[24]	Wedepohl K H. The composition of the continental crust[J]. Geochimica et Cosmochimica Acta, 1995, 59(7):1217-1232.
[25]	周向斌, 李剑锋, 王可勇, 等. 吉林延边五星山-五凤金矿床碱长花岗岩锆石U-Pb定年及其地质意义[J]. 大地构造与成矿学, 2016, 40(6):1215-1225. Zhou X B, Li J F, Wang K Y, et al. LA-ICP-MS zircon U-Pb dating of alkali granite in Wuxingshan-wufeng gold deposit in Yanbian area, Jilin Province and its geological significance[J]. Geotectonica et Metallogenia, 2016, 40(6):1215-1225.
[26]	赵振华. 微量元素地球化学原理[M]. 北京:科学出版社, 1997: 71-73, 122. Zhao Z H. Principle of trace element geochemistry[M]. Beijing: Science Press, 1997:71-73,122. (in Chinese)
[27]	Barth M G, McDonough W F, Rudnick R L. Tracking the budget of Nb and Ta in the continental crust[J]. Chemical Geology, 2000, 165(3/4):197-213.
[28]	Gao S, Luo T C, Zhang B R, et al. Chemical composition of the continental crust as revealed by studies in East China[J]. Geochimica et Cosmochimica Acta, 1998, 62(11):1959-1975.
[29]	Furukawa Y, Tatsumi Y. Melting of a subducting slab and production of high-Mg andesite magmas:Unusual magmatism in SW Japan at 13-15 Ma[J]. Geophysical Research Letters, 1999, 26(15):2271- 2274.
[30]	Kamei A, Owada M, Nagao T, et al. High-Mg diorites derived from sanukitic HMA magmas, Kyushu Island, southwest Japan arc: Evidence from clinopyroxene and whole rock compositions[J]. Lithos, 2004, 75(3/4):359-371.
[31]	Mazzeo F C, D'Antonio M, Arienzo I, et al. Subduction-related enrichment of the Neapolitan volcanoes (Southern Italy) mantle source:New constraints on the characteristics of the slab-derived components[J]. Chemical Geology, 2014, 386:165-183.
[32]	Santosh M, Teng X M, He X F, et al. Discovery of Neoarchean suprasubduction zone ophiolite suite from Yishui complex in the North China Craton[J]. Gondwana Research, 2016, 38:1-27.
[33]	Deng J, Wang C M, Bagas L, et al. Crustal architecture and metallogenesis in the south-eastern North China Craton[J]. Earth- Science Reviews, 2018, 182:251-272.
[34]	Yang F, Santosh M, Kim S W. Mesozoic magmatism in the eastern North China Craton:insights on tectonic cycles associated with progressive craton destruction[J]. Gondwana Research, 2018, 60: 153-178.
[35]	Jahn B M, Wu F Y, Lo C H, et al. Crust-mantle interaction induced by deep subduction of the continental crust:Geochemical and Sr-Nd isotopic evidence from post-collisional mafic-ultramafic intrusions of the northern Dabie complex, central China[J]. Chemical Geology, 1999, 157(1/2):119-146.
[36]	La Flèche M R, Camiré G, Jenner G A. Geochemistry of post- Acadian, Carboniferous continental intraplate basalts from the Maritimes Basin, Magdalen Islands, Québec, Canada[J]. Chemical Geology, 1998, 148(3/4):115-136.
[37]	Atherton M P, Petford N. Generation of sodium-rich magmas from newly underplated basaltic crust[J]. Nature, 1993, 362(6416): 144-146.
[38]	Schiano P, Monzier M, Eissen J P, et al. Simple mixing as the major control of the evolution of volcanic suites in the Ecuadorian Andes [J]. Contributions to Mineralogy and Petrology, 2010, 160(1):297- 312.
[39]	Turner S, Caulfield J, Turner M, et al. Recent contribution of sediments and fluids to the mantle's volatile budget[J]. Nature Geoscience, 2012, 5(1):50-54.
[40]	赵春荆, 彭玉鲸, 党增欣, 等. 吉黑东部构造格架及地壳演化[M]. 沈阳:辽宁大学出版社, 1996:1-186. Zhao C J, Peng Y J, Dang Z X, et al. Tectonic framework and crust evolution of Eastern Jilin and Heilongjiang Provinces[M]. Shenyang: Liaoning University Press, 1996:1-186.
[41]	彭玉鲸, 齐成栋, 周晓东, 等. 吉黑复合造山带古亚洲洋向滨太平洋构造域转换[J]. 地质与资源, 2012, 21(3):261-265. Peng Y J, Qi C D, Zhou X D, et al. Transition from Paleo-Asian Ocean domain to circum-Pacific Ocean domain for the Ji-Hei composite orogenic belt:Time mark and relationship to global tectonics[J]. Geology and Resources, 2012, 21(3):261-265.
[42]	Xu W L, Ji W Q, Pei F P, et al. Triassic volcanism in eastern Heilongjiang and Jilin provinces, NE China:Chronology, geochemistry, and tectonic implications[J]. Journal of Asian Earth Sciences, 2009, 34(3):392-402.
[43]	Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic granitoids in northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41(1):1-30.
[44]	Condie K C. Geochemical changes in basalts and andesites across the Archean-Proterozoic boundary:Identification and significance[J]. Lithos, 1989, 23(1/2):1-18.
[45]	Pearce J A, Norry M J. Petrogenetic implications of Ti, Zr, Y, and Nb variations in volcanic rocks[J]. Contributions to Mineralogy and Petrology, 1979, 69(1):33-47.
[46]	Zhang S H, Zhao Y, Davis G A, et al. Temporal and spatial variations of Mesozoic magmatism and deformation in the North China Craton:Implications for lithospheric thinning and decratonization[J]. Earth-science Reviews, 2014, 131:49-87.